Aeolian imprints of multiple Mediterranean invasions of the Black Sea during Pleistocene

Basit Öğe Kaydı
dc.authorid0000-0002-3112-5258
dc.authorid0000-0001-7629-5747
dc.authorid0000-0002-9834-7680
dc.authorid0000-0001-8704-4935
dc.authorid0000-0002-1084-0180
dc.authorid0000-0001-8598-8596
dc.authorid0000-0002-9972-429X
dc.contributor.authorErginal, Ahmet Evrenen_US
dc.contributor.authorGüneç Kıyak, Nafiyeen_US
dc.contributor.authorMakaroğlu, Özlemen_US
dc.contributor.authorBozcu, Mustafaen_US
dc.contributor.authorÖztürk, Muhammed Zeynelen_US
dc.contributor.authorSelim, Haluk Hamiten_US
dc.contributor.authorNowacyzk, Norbert R.en_US
dc.contributor.authorKaya, Nurcanen_US
dc.contributor.authorÖztürk, Tuğbaen_US
dc.contributor.authorKarabıyıkoğlu, Mustafaen_US
dc.contributor.authorPolymeris, Georgios S.en_US
dc.date.accessioned2022-04-05T18:08:43Z
dc.date.available2022-04-05T18:08:43Z
dc.date.issued2022-03-04
dc.departmentIşık Üniversitesi, Fen Edebiyat Fakültesi, Fizik Bölümüen_US
dc.departmentIşık University, Faculty of Arts and Sciences, Department of Physicsen_US
dc.descriptionThis work was supported by the Scientific and Technological Research Council of Turkey (TUBITAK; project number: 113Y418 ) and the Turkish Academy of Sciences (TUBA). We would like to thank Mustafa Avcıoğlu, Çağlar Çakır, Emrah Özpolat, Hakan Kaya and Abdullah Akbaş for their assistance in the field studies. Graham Lee is thanked for his help in correcting the English text of the article. We are honoured to dedicate this study in loving memory of the great Turkish Geographer, Professor Oğuz Erol, who passed away on April 11, 2014.en_US
dc.description.abstractClimate changes determined the repeated connections between the Black Sea, Caspian Sea and Mediterranean Sea. The landlocked anoxic Black Sea basin was exposed to several transgressions throughout Quaternary by the Mediterranean Sea through the Straits of Istanbul (Bosphorus) and by the Caspian Sea through the Manych-Kerch spillway. Sedimentological records of these connections are limited mostly to the marine terrace deposits of Marine Isotope Stage (MIS) 5e while the pre-MIS 5e period remains uncertain due to a lack of robust facies and chronological data from deep-sea sedimentary sequences. Here we discuss the imprints of multiple Mediterranean transgressions during Middle Pleistocene in the Black Sea based on facies analysis and the optical age of coastal carbonate aeolianites. Contrary to today's hydro-climate of the Black Sea, the aeolianites bear witness to the transformation of the Black Sea into a warm inland sea during successive Mediterranean invasions. Prior to the onset of aeolian deposition, paleosols were formed on the Eocene-aged hardened sandy silts, suggesting strongly washed soil. This is evidenced by no calcium carbonate and a high Rb/Sr ratio, with quartz amounting to of 99.8%. According to our OSL ages, carbonates deposited on the shelf plain under higher temperature and increased evaporation conditions in MIS 15 and the later interglacial phases were transported to the coastal sand dunes during the transitional phases of MIS 15–14, MIS 13–12, MIS 11–10 and MIS 9–8. We suggest that the carbonate-rich and ooid-containing aeolianites were repeatedly formed in the multiple Mediterranean transgression stages, beginning with an increasingly severe dry phase following the Brunhes-Matuyama magnetic reversal.en_US
dc.description.sponsorshipTürkiye Bilimsel ve Teknolojik Araştırma Kurumu (TÜBİTAK)en_US
dc.description.sponsorshipTurkish Academy of Sciences (TUBA)en_US
dc.description.versionPublisher's Versionen_US
dc.identifier.citationErginal, A. E., Güneç Kıyak, N., Makaroğlu, Ö., Bozcu, M., Öztürk, M. Z., Selim, H. H., Nowacyzk, N. R., Kaya, N., Öztürk, T., Karabıyıkoğlu, M. & Polymeris, G. S. (2022). Aeolian imprints of multiple Mediterranean invasions of the Black Sea during Pleistocene. Palaeogeography, Palaeoclimatology, Palaeoecology, 592, 1-14. doi:10.1016/j.palaeo.2022.110902en_US
dc.identifier.doi10.1016/j.palaeo.2022.110902
dc.identifier.endpage14
dc.identifier.issn0031-0182
dc.identifier.issn1872-616X
dc.identifier.scopus2-s2.0-85125695979
dc.identifier.scopusqualityQ1
dc.identifier.startpage1
dc.identifier.urihttps://hdl.handle.net/11729/3856
dc.identifier.urihttp://dx.doi.org/10.1016/j.palaeo.2022.110902
dc.identifier.volume592
dc.identifier.wosWOS:000971464700001
dc.identifier.wosqualityQ1
dc.indekslendigikaynakWeb of Scienceen_US
dc.indekslendigikaynakScopusen_US
dc.indekslendigikaynakScience Citation Index Expanded (SCI-EXPANDED)en_US
dc.institutionauthorÖztürk, Tuğbaen_US
dc.institutionauthorid0000-0001-8598-8596
dc.language.isoenen_US
dc.peerreviewedYesen_US
dc.publicationstatusPublisheden_US
dc.publisherElsevier B.V.en_US
dc.relation.ispartofPalaeogeography, Palaeoclimatology, Palaeoecologyen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectBlack Seaen_US
dc.subjectCarbonate aeolianiteen_US
dc.subjectClimate changeen_US
dc.subjectInterglacialen_US
dc.subjectMarine isotope stagesen_US
dc.subjectOoiden_US
dc.subjectPaleosolen_US
dc.subjectBosporus Straiten_US
dc.subjectCaspian Seaen_US
dc.subjectIstanbulen_US
dc.subjectMediterranean Seaen_US
dc.subjectBearen_US
dc.subjectCalcium carbonateen_US
dc.subjectEvaporationen_US
dc.subjectFacies analysisen_US
dc.subjectInland seaen_US
dc.subjectPleistoceneen_US
dc.subjectQuaternaryen_US
dc.subjectTransformationen_US
dc.subjectTransgressionen_US
dc.subjectSharon coastal-plainen_US
dc.subjectLord-howe-islanden_US
dc.subjectLevel highstand
dc.subjectSingle-aliquoten_US
dc.subjectLuminescence chronology
dc.subjectDose-rateen_US
dc.subjectQuaternary stratigraphyen_US
dc.subjectMiddle Pleistoceneen_US
dc.subjectWestern-Australiaen_US
dc.subjectMessinian eventen_US
dc.titleAeolian imprints of multiple Mediterranean invasions of the Black Sea during Pleistoceneen_US
dc.typeArticleen_US
dspace.entity.typePublication

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